摘要
Three relatively large intrusions locating in Fanchang district,the Lower Yangtze region,are Banshiling,Fushan and Binjiang plutons,rock types of which are dominantly quartz-monzonite,potassium feldspar granite and granite,respectively.Zircon LA-ICPMS U-Pb dating of three intrusions give quite accordant ages of (124.9±1.7) Ma, (126.4±1.7) Ma,(124.6±4.7) Ma (the coarse-grained phase of Binjiang pluton) and (123.0±1.8) Ma (the fine-grained phase of Binjiang pluton),respectively. The petrogenesis and magmatic source of the three stage magmatism in the Lower Yangtze region reveal a clearly deep geological process of evolution under an extension setting with increasing intensity during three magmatic stages.